標(biāo)題: Titlebook: Dynamic Processes in the Chemistry of the Upper Ocean; J. D. Burton,P. G. Brewer,R. Chesselet Book 1986 Springer Science+Business Media Ne [打印本頁(yè)] 作者: Gram114 時(shí)間: 2025-3-21 17:36
書目名稱Dynamic Processes in the Chemistry of the Upper Ocean影響因子(影響力)
書目名稱Dynamic Processes in the Chemistry of the Upper Ocean影響因子(影響力)學(xué)科排名
書目名稱Dynamic Processes in the Chemistry of the Upper Ocean網(wǎng)絡(luò)公開度
書目名稱Dynamic Processes in the Chemistry of the Upper Ocean網(wǎng)絡(luò)公開度學(xué)科排名
書目名稱Dynamic Processes in the Chemistry of the Upper Ocean被引頻次
書目名稱Dynamic Processes in the Chemistry of the Upper Ocean被引頻次學(xué)科排名
書目名稱Dynamic Processes in the Chemistry of the Upper Ocean年度引用
書目名稱Dynamic Processes in the Chemistry of the Upper Ocean年度引用學(xué)科排名
書目名稱Dynamic Processes in the Chemistry of the Upper Ocean讀者反饋
書目名稱Dynamic Processes in the Chemistry of the Upper Ocean讀者反饋學(xué)科排名
作者: MENT 時(shí)間: 2025-3-22 00:11 作者: rods366 時(shí)間: 2025-3-22 00:59
Surface Water 234Th/238U Disequilibria: Spatial and Temporal Variations of Scavenging Rates within td with particulate organic carbon flux throughout a wide range of marine environments ranging from estuaries to the deep sea. Including these environments, which represent end-members for .Th scavenging intensity, the residence time for dissolved .Th is shown to vary from 0.3 days to 2 years dependi作者: Pastry 時(shí)間: 2025-3-22 05:13
Dominant Microorganisms of the Upper Ocean: Form and Function, Spatial Distribution and Photoregulat dominant microorganisms have two major distributions, as plankters free in the water and as epibionts associated with the aggregated seston that makes up marine snow. Their physical state as plankters or as epibionts has a major effect on their spatial distribution and, therefore, their activity an作者: critique 時(shí)間: 2025-3-22 11:13
What Controls the Variability of Carbon Dioxide in the Surface Ocean? A Plea for Complete Informatio those invoking the dominance of physical processes..What appears to be true is that a complete experiment separating these effects has yet to be done, recognizing that the feedback between ocean mixing and biological productivity prevents, of course, a truly separate set of processes. The great var作者: 掙扎 時(shí)間: 2025-3-22 15:05
Gustav Fr?lich,Walter Sp?ttel,Ernst T?nzero for the marine atmosphere. Such processes include air-sea exchange of stable gases and particles, as well as free radicals and other unstable species. Furthermore, biological and photochemical activity near the ocean surface leads to the production of gases and to speciation changes for ionic form作者: 掙扎 時(shí)間: 2025-3-22 18:18 作者: nominal 時(shí)間: 2025-3-22 23:17
Bernhard Kirschstein,Floris Koppelmannd with particulate organic carbon flux throughout a wide range of marine environments ranging from estuaries to the deep sea. Including these environments, which represent end-members for .Th scavenging intensity, the residence time for dissolved .Th is shown to vary from 0.3 days to 2 years dependi作者: Ptosis 時(shí)間: 2025-3-23 01:55
Bernhard Kirschstein,Floris Koppelmann dominant microorganisms have two major distributions, as plankters free in the water and as epibionts associated with the aggregated seston that makes up marine snow. Their physical state as plankters or as epibionts has a major effect on their spatial distribution and, therefore, their activity an作者: Anthrp 時(shí)間: 2025-3-23 08:48
Werner Nagel,Elisabeth Brandenburger those invoking the dominance of physical processes..What appears to be true is that a complete experiment separating these effects has yet to be done, recognizing that the feedback between ocean mixing and biological productivity prevents, of course, a truly separate set of processes. The great var作者: 下船 時(shí)間: 2025-3-23 10:26 作者: 侵略 時(shí)間: 2025-3-23 15:40
a somewhat different emphasis emerged, focused on the question as to how chemists should set about observing an environment as variable and dynamic as the upper ocean and selecting the appropriate scales for the framework of measurements to study a particular process, especially in the light of current knowl978-1-4684-5217-4978-1-4684-5215-0作者: FID 時(shí)間: 2025-3-23 19:46 作者: Ataxia 時(shí)間: 2025-3-23 22:41 作者: Diatribe 時(shí)間: 2025-3-24 05:40 作者: 仔細(xì)檢查 時(shí)間: 2025-3-24 07:17 作者: 反對(duì) 時(shí)間: 2025-3-24 12:43 作者: GOAT 時(shí)間: 2025-3-24 17:34 作者: 智力高 時(shí)間: 2025-3-24 20:48
Die physikalischen Eigenschaften der Wollethe Californian coast have been examined from the process-oriented perspective of space and time scale analysis. In this region of the ocean, upwelling, offshore mesoscale eddies and large-scale “El Ni?o”-type processes dominate. Each of these physical processes has a velocity field which transports作者: 放肆的我 時(shí)間: 2025-3-25 03:14
Die Wirbelstromverluste im Massekernhe processes responsible for the observed changes. The research program was multi-disciplinary and included components from physical, biological and chemical oceanography, remote sensing, and mathematical modeling. This report focuses on the physical structure of warm-core rings and its change with 作者: employor 時(shí)間: 2025-3-25 05:15
Ferdinand Trendelenburg,Erich Franzidentified as the cumulative effect of fluctuations in the velocity components combined with fluctuations in the concentrations. Recent work enables the vertical eddy diffusivity coefficient to be parameterized in terms of small scale parameters for two portions of the water column; the region just 作者: 依法逮捕 時(shí)間: 2025-3-25 08:53 作者: Repetitions 時(shí)間: 2025-3-25 14:04
Ragnar Holm,Bernhard Kirschsteinany gases, the transfer between the interface and the bulk liquid (transfer coefficient k.) is rate controlling, whereas for other gases, notably reactive ones, a more complex situation has to be dealt with. The available oceanic field data for k. are presented. The value of k. increases considerabl作者: FER 時(shí)間: 2025-3-25 18:25
Die Raumladungsschw?chung des Schroteffektesc processes. The ozone influx is probably the largest and most significant one. Ozone reacts with dissolved iodide and with other unknown components. One consequence is the formation of volatile iodine species, perhaps in sufficient amounts to balance the atmospheric iodine budget. However, most of 作者: 過度 時(shí)間: 2025-3-25 20:50 作者: CALL 時(shí)間: 2025-3-26 00:29
Bernhard Kirschstein,Floris Koppelmannimes, ranged from oligotrophic subtropical gyres to eutrophic eastern boundary and equatorial divergence zones. Modeling of the disequilibria between .Th and .U within the surface waters provides estimates for the residence time of dissolved thorium with respect to particle scavenging, the residence作者: 專橫 時(shí)間: 2025-3-26 05:44
Bernhard Kirschstein,Floris Koppelmann, but are so numerous that a 3 or 30 ml sample yields a statistically significant count of the bacteria and flagellates, respectively. The bacterial population contains not only the organotrophs responsible for organic matter decomposition and mineralization, but conspicuous and important population作者: mettlesome 時(shí)間: 2025-3-26 10:53 作者: heckle 時(shí)間: 2025-3-26 16:08
Die Raumladungsschw?chung des Schroteffekteserently intricate and are variable in time and space due to environmental dependencies. Modeling provides a mechanism by which complex biological-environmental interactions can be studied. This potential is evident in the progress exhibited in the construction of biological-physical subsystem models作者: 小母馬 時(shí)間: 2025-3-26 20:35 作者: opinionated 時(shí)間: 2025-3-26 21:37 作者: 元音 時(shí)間: 2025-3-27 02:24
Nato Conference Serieshttp://image.papertrans.cn/e/image/283715.jpg作者: Aqueous-Humor 時(shí)間: 2025-3-27 06:42 作者: Musculoskeletal 時(shí)間: 2025-3-27 10:57
Report of Working Group III: SolutesThe majority of analyses made up to the present distinguish the dissolved and particulate phases by means of filtration using a pore size of about 0.4 μm. This may not be appropriate, particularly if colloidal or bacterial particles are of importance.作者: neutralize 時(shí)間: 2025-3-27 13:43 作者: sundowning 時(shí)間: 2025-3-27 20:57
https://doi.org/10.1007/978-1-4684-5215-0Pacific Ocean; chemistry; environment; marine; marine science; ocean; research; transport作者: 枕墊 時(shí)間: 2025-3-28 00:33 作者: STERN 時(shí)間: 2025-3-28 02:08 作者: ANA 時(shí)間: 2025-3-28 06:44 作者: 熒光 時(shí)間: 2025-3-28 11:10 作者: 符合國(guó)情 時(shí)間: 2025-3-28 18:25
Upper Ocean Chemistry: Space and Time Scalesep ocean. The complexity and variability of the upper layers of the ocean at a wide range of space and time scales has been demonstrated by the dense sampling techniques available for temperature, salinity and chlorophyll. It is highly probable that for many chemical constituents there will be simil作者: Emmenagogue 時(shí)間: 2025-3-28 22:31
The Chemistry of Near-Surface Seawaters almost impossible to define in a meaningful way, and microlayer thicknesses are by default specified in terms of what the various sampling devices appear to collect. The organic composition of the microlayer is poorly characterized and its study suffers from similar problems to analogous work in b作者: Banister 時(shí)間: 2025-3-28 23:16
Processes Affecting Upper Ocean Chemical Structure in an Eastern Boundary Currentthe Californian coast have been examined from the process-oriented perspective of space and time scale analysis. In this region of the ocean, upwelling, offshore mesoscale eddies and large-scale “El Ni?o”-type processes dominate. Each of these physical processes has a velocity field which transports作者: maintenance 時(shí)間: 2025-3-29 07:01 作者: 開始從未 時(shí)間: 2025-3-29 10:08 作者: 我不死扛 時(shí)間: 2025-3-29 14:18
Convection in the Upper Oceanan occur just below the sea surface whenever there is a transfer of heat from the ocean to the atmosphere. The horizontal scale of this convection will typically be a few centimetres. Usually this convection will be intermittent with a characteristic period of the order of a minute. The small scale 作者: abduction 時(shí)間: 2025-3-29 15:51 作者: 東西 時(shí)間: 2025-3-29 20:49 作者: 轎車 時(shí)間: 2025-3-30 00:25 作者: Cabinet 時(shí)間: 2025-3-30 07:15 作者: Coronation 時(shí)間: 2025-3-30 09:50 作者: 大約冬季 時(shí)間: 2025-3-30 12:28
Short Term Variations in Primary Productivitye for ocean chemistry and physics. The first concerns implications, for studies of mixing in the surface layer, of the fact that phytoplankton “remember” their past light history. Here time scales of minutes to hours are important. The second concerns primary production as the driving force for the 作者: 根除 時(shí)間: 2025-3-30 20:24
Some Perspectives on Ecological Modeling Focused on Upper Ocean Processeserently intricate and are variable in time and space due to environmental dependencies. Modeling provides a mechanism by which complex biological-environmental interactions can be studied. This potential is evident in the progress exhibited in the construction of biological-physical subsystem models作者: Spangle 時(shí)間: 2025-3-30 23:34
What Controls the Variability of Carbon Dioxide in the Surface Ocean? A Plea for Complete Informatio, are among the most important problems addressed by ocean chemists today..There is wide agreement as to experimental procedures in this field, through the measurement of alkalinity, total CO., pH and pCO. of ocean waters, together with physical properties and .C. Moreover the uncertainties surround作者: PAEAN 時(shí)間: 2025-3-31 01:23 作者: judiciousness 時(shí)間: 2025-3-31 07:52 作者: 我邪惡 時(shí)間: 2025-3-31 12:41
Ragnar Holm,Friedrich Güldenpfennigo acids, thiols, low molecular weight carbonyl compounds, carboxylic acids, and metal-organic complexes. Emphasis is placed on how the methods work, their limitations, and examples of field applications.作者: 翅膀拍動(dòng) 時(shí)間: 2025-3-31 15:10
Upper Ocean Chemistry: Space and Time Scales to give comparable density of observation in the three dimensions x, z & t, (2) Relations between selected organic compounds which may have large coherence scales as a result of their specific biological functions, and (3) Integration of surface and deep water studies, particularly, but not solely, through the use of sediment trap methods.作者: Constrain 時(shí)間: 2025-3-31 20:43
Organic Chemical Dynamics of the Mixed Layer: Measurement of Dissolved Hydrophilic Organics at Seao acids, thiols, low molecular weight carbonyl compounds, carboxylic acids, and metal-organic complexes. Emphasis is placed on how the methods work, their limitations, and examples of field applications.作者: 赤字 時(shí)間: 2025-4-1 01:05
Report of Working Group I: Gasesre (e.g., CO, NO, N.O). In some instances (e.g., (CH.).S, CH.I) the fluxes from the ocean to the atmosphere make significant contributions to the global cycling of the elements, and in others (e.g., CO.) the flux into the ocean exerts an important control on atmospheric composition.
